Input of 87Sr/86Sr ratios and Sr geochemical signatures to update knowledge on thermal and mineral waters flow paths in fractured rocks (N-Portugal)

Author:

Marques J.M.,Carreira P.M.,Goff F.,Eggenkamp H.G.M.,Antunes da Silva M.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Pollution,Environmental Chemistry

Reference45 articles.

1. Elemental and isotopic geochemistry in the hydrothermal area of Chaves/Vila Pouca de Aguiar (Northern Portugal);Aires-Barros;Environ. Geol.,1995

2. Hot and cold CO2-rich mineral waters in Chaves geothermal area (northern Portugal);Aires-Barros;Geothermics,1998

3. Andrade, M.P.L., 2003. The isotope geochemistry of thermomineral water. Contribution of the isotopes of Sr (87Sr/86Sr) and Cl (37Cl/35Cl) in the development of circulation models. The case of some carbon dioxide waters in N Portugal. Unpublished MSc Thesis, Instituto Superior Técnico, Technical Univ. Lisbon, Lisbon (in Portuguese).

4. Baptista, J., Coke, C., Dias, R., Ribeiro, A., 1993. Tectonics and geomorphology of Pedras Salgadas region and associated mineral springs. In: Chambel, A. (Ed.), Comunicações da XII Reunião de Geologia do Oeste Peninsular, vol. 1. Évora University, pp. 125–139 (in Portuguese).

5. 87Sr/86Sr ratios of Sierra Nevada stream waters: implications for relative mineral weathering rates;Blum;Geochim. Cosmochim. Acta,1994

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